Bo Holm Jacobsen

TL;DR: In this paper, the upward continuation operator is given by elementary functions in both space and wavenumber domains, and is numerically stable, and also physically comprehensible when applied to real, nonrandom anomalies.

TL;DR: It is shown that distinct, ∼55- to 70-year oscillations characterized the North Atlantic ocean-atmosphere variability over the past 8,000 years, and that the coupling from the AMO to regional climate conditions was modulated by orbitally induced shifts in large-scale ocean- atmosphere circulation.

TL;DR: In this article, a laterally constrained inversion scheme for continuous resistivity data based on a layered earth model (1D) is presented, where all 1D data sets and models are inverted as one system, producing layered sections with lateral smooth transitions.

TL;DR: In this article, a model of protracted exhumation of topography since the Caledonide Orogeny is presented, which can be substantially explained by the evidence that the evidence can be reasonably explained by a model that the topography of western Scandinavia was created by some form of active tectonic uplift during the Cenozoic.

TL;DR: The evidence suggests that external forcing played a dominant role in pacing the AMO after termination of the Little Ice Age, with an instantaneous impact on mid-latitude sea-surface temperatures that spread across the North Atlantic over the ensuing ~5 years.